中亚热带常绿阔叶林不同演替阶段木质残体碳密度特征

doi:10.13466/j.cnki.lyzygl.2014.02.013

林业资源管理 ›› 2014, Vol. 0 ›› Issue (2): 66-72.doi: 10.13466/j.cnki.lyzygl.2014.02.013

中亚热带常绿阔叶林不同演替阶段木质残体碳密度特征

曾掌权^1,2,3, 汪思龙^2,3, 张灿明¹, 吴子剑¹, 李锡泉¹, 罗佳¹

1.湖南省林业科学院国家林业局湖南衡山森林生态系统定位观测研究站,长沙 410004;
2.中国科学院会同森林生态实验站,森林与土壤生态国家重点实验室,中国科学院沈阳应用生态研究所,沈阳 110164;
3.湖南会同森林生态系统国家野外科学观测研究站,湖南会同 418307

收稿日期:2014-01-22 修回日期:2014-04-22 出版日期:2014-04-28 发布日期:2020-12-09
通讯作者: 汪思龙(1964-),男,安徽池州人,研究员,主要从事森林碳氮循环的研究工作。Email:slwang@iae.ac.cn
作者简介:曾掌权(1976-),男,湖南益阳人,助理研究员,博士,主要从事森林生态功能的研究工作。Email:zengzquan@163.com
基金资助:
科技部国家国际科技合作专项项目(2012DFB30030);湖南省林业科学院青年科研创新基金(2013LQJ08,2013LQJ11);“十二五”环境领域国家科技计划课题(2012BAC09B03-4);中科院先导科技专项(XDA05050205);国家林业局948项目(2009-4-46)。

Carbon Storage of Woody Debris of Evergreen Broad-leaf Forests in Mid-subtropical Region of China at Three Succession Stages

ZENG Zhangquan^1,2,3, WANG Silong^2,3, ZHANG Canming¹, WU Zijian¹, LI Xiquan¹, LUO Jia¹

1. Hunan Academy of Forestry,Hengshan Research Station of Forest Ecosystem,Changsha 410004,China;
2. Huitong Experimental Station of Forest Ecology,State Key Laboratory of Forest and Soil Ecology,Institute of Applied Ecology,Chinese Academy of Sciences,Shenyang 110164,China;
3. Huitong National Research Station of Forest Ecosystem,Huitong,Hunan 418307,China

Received:2014-01-22 Revised:2014-04-22 Online:2014-04-28 Published:2020-12-09

摘要/Abstract

摘要： 为了更好地了解常绿阔叶林恢复演替过程中木质残体(WD)碳储量的变化特征,对鹰嘴界马尾松林、针阔混交林、常绿阔叶林进行了调查取样,结果表明:鹰嘴界常绿阔叶林演替阶段各林分中木质残体的现存量较低,在1.26～8.82 Mg/hm²之间,大小顺序为马尾松林<针阔混交林<常绿阔叶林,随演替进程呈逐渐增加趋势;演替阶段粗木质残体(CWD)碳含量因树种及其分解等级而异,随着CWD分解等级的提高,其碳含量逐渐降低;马尾松林、针阔混交林和常绿阔叶林的木质残体碳密度分别为0.62,1.75,3.78 Mg/hm²,分别相当于各林分乔木层碳密度的0.73%、1.83%和2.92%。

关键词: 木质残体, 碳储量, 常绿阔叶林, 中亚热带, 演替阶段

Abstract: To better understand the effect of forest succession on carbon storage of woody debris(WD),carbon stock and allocation of evergreen broadleaf forest,a major zonal forest in subtropical China was investigated.Three forest types were sampled,i.e.,pine(Pinus massoniana)forest(PF),pine and broadleaf mixed forest(MF)and evergreen broadleaf forest(BF).The amount of woody debris(WD)biomass was between 1.26-8.82 Mg/hm²,in the following order:PF<MF<BF,which showed a trend of increase gradually with the succession.Coarse woody debris(CWD)carbon content varies with tree species and its decomposition level,with the improvement of CWD decomposition level,its carbon content gradually decreases.The woody debris carbon storages of PF,MF,and BF were 0.62 Mg/hm²,1.75 Mg/hm² and 3.78 Mg/hm²,respectively,corresponding to 0.73%,1.83% and 2.92% of the tree carbon storage.

Key words: woody debris, carbon storage, evergreen broad-leaf forests, mid-subtropical region, succession

中图分类号:

曾掌权, 汪思龙, 张灿明, 吴子剑, 李锡泉, 罗佳. 中亚热带常绿阔叶林不同演替阶段木质残体碳密度特征[J]. 林业资源管理, 2014, 0(2): 66-72.

ZENG Zhangquan, WANG Silong, ZHANG Canming, WU Zijian, LI Xiquan, LUO Jia. Carbon Storage of Woody Debris of Evergreen Broad-leaf Forests in Mid-subtropical Region of China at Three Succession Stages[J]. FOREST RESOURCES WANAGEMENT, 2014, 0(2): 66-72.

参考文献

[1]杨玉盛,郭剑芬,林鹏,等.格氏栲天然林与人工林粗木质残体碳库及养分库[J].林业科学,2005,41(3):7-11.
[2]Brown S.Measuring carbon in forests:Current status and future challenges [J].Environmental Pollution,2002,116:362-372.
[3]Wilcke W,Hess T,Bengel C,et al.Coarse woody debris in a montane forest in Ecuador:Mass C and nutrient stock and turnover[J].Forest Ecology and Management,2005,205:139-147.
[4]Harmon M E,Franklin J F,Swanson F J,et al.The ecology of coarse woody debris in temperate ecosystems [J].Advances in Ecological Research,1986.15:133-302.
[5]Sturtevant B R,Bissonette J A,Long J N,et al.Coarse woody debris as a function of age,stand structure,and disturbance in boreal Newfoundland [J].Ecological Applications,1997,7:702-712.
[6]唐旭利,周国逸.亚热带典型森林演替类型粗死木质残体贮量及其对碳循环的潜在影响[J].植物生态学报,2005,29(4):559-568.
[7]Kapeluck P R.Coarse woody debris in an age sequence of southern Appalachian forests[D].Clemson University,2002.
[8]李凌浩,邢雪荣,黄大明,等.武夷山甜储林粗死木质残体的贮量、动态及其功能评述[J].植物生态学报,1996,24(2):132-143.
[9]唐旭利,周国逸,周霞,等.鼎湖山季风常绿阔叶林粗死木质残体的研究[J].植物生态学报,2003,27(4):484-489.
[10]高甲荣,王敏,毕利东,等.贡嘎山不同年龄结构峨眉冷杉林粗木质残体的贮存量及其特征[J].中国水土保持科学,2003,1(2):47-50.
[11]袁正科,林柏.湖南鹰嘴界自然保护区科考报告[M].2003.
[12]Zeng Zhangquan,Wang Silong,Zhang Canming,et al.The carbon storage of evergreen broad-leaf forests in mid-subtropical region of China at four succession stages[J].Journal of Forestry Research,2013,24(4):677-682.
[13]Maser C,Trappe J M,Nussbaum R A.Fungal small mammal interrelationships with emphasis on Oregon coniferous forests [J].Ecology,1978,59:799-809.
[14]Pyle C,Brown M M.Heterogeneity of wood decay classes within hardwood logs [J].Forest Ecology and Management,1999,114:253-259.
[15]杨礼攀,刘文耀,杨国平,等.哀牢山湿性常绿阔叶林和次生林木质物残体的组成与碳贮量[J].应用生态学报,2007,18(10):2153-2159.
[16]Liu Wenyao,John ED Fox,Xu Zaifu.Biomass and nutrient accumulation in montane evergreen broad-leaved forest(Lithocarpus xylocarpus type)in Ailao Mountains,SW China [J].Forest Ecology and Management,2002,158:223-235.
[17]Carmona R C,Juan J A,Juan C A,et al.Coarse woody debris biomass in successional and primary temperate forests in Chiloe Island,Chile [J].Forest Ecology and Management,2002,164:265-275.
[18]Schroeder P E,Winjum J K.Assessing Brazil’s carbon budget:I.Biotic carbon pools [J].Forest Ecology and Management,1995,75:77-86.

中亚热带常绿阔叶林不同演替阶段木质残体碳密度特征

Carbon Storage of Woody Debris of Evergreen Broad-leaf Forests in Mid-subtropical Region of China at Three Succession Stages

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